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Epipelagic mesozooplankton distribution and abundance over the Mascarene Plateau and Basin, south-western Indian Ocean
Gallienne, C.P.; Conway, D.V.P.; Robinson, J.; Naya, N.; William, J.S.; Lynch, T.; Meunier, S. (2004). Epipelagic mesozooplankton distribution and abundance over the Mascarene Plateau and Basin, south-western Indian Ocean. J. Mar. Biol. Ass. U.K. 84(1): 1-8. https://dx.doi.org/10.1017/S0025315404008835h
In: Journal of the Marine Biological Association of the United Kingdom. Cambridge University Press/Marine Biological Association of the United Kingdom: Cambridge. ISSN 0025-3154; e-ISSN 1469-7769
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| Trefwoorden |
Abundance
Aquatic communities > Plankton > Zooplankton
Distribution
ISW, Indian Ocean
ISW, Mascarene Basin
Population characteristics > Biomass
Copepoda [WoRMS]; Harpacticoida [WoRMS]
Indische Oceaan [Marine Regions]; Mascarene Basin [Marine Regions]
Marien/Kust |
| Auteurs | | Top |
- Gallienne, C.P.
- Conway, D.V.P.
- Robinson, J.
- Naya, N.
|
- William, J.S.
- Lynch, T.
- Meunier, S.
|
|
| Abstract |
The crescent shaped Mascarene Plateau (south-western Indian Ocean), some 2200 km in length, forms a partial barrier to the (predominantly westward) flow of the South Equatorial Current. Shallow areas of the Mascarene Plateau effectively form a large shelf sea without an associated coastline. Zooplankton sampling transects were made across the plateau and also the basin to the west, to investigate the role the partial interruption of flow has on zooplankton biomass and community structure over the region. Biomass data from optical plankton counter (OPC) analysis, and variability in community structure from taxonomic analysis, appear to indicate that the obstruction by the plateau causes upwelling, nutrient enrichment and enhanced chlorophyll and secondary production levels downstream. The Mascarene Basin is clearly distinguishable from the ridge itself, and from the waters to the south and north, both in terms of size-distributed zooplankton biomass and community structure. Satellite remote sensing data, particularly remotely-sensed ocean colour imagery and the sea surface height anomaly (SSHA), indicate support for this effect. A correlation was found between OPC biovolume and SSHA and sea surface temperature (SST), which may indicate the physical processes driving mesozooplankton variability in this area. Biomass values away from the influence of the ridge averaged 24 mg m−3, but downstream of the ridge biomass averaged 263 mg m−3. Copepods comprised 60% of the mean total organisms. Calanoid copepod numbers varied considerably between regions, being lowest away from the influence of the plateau, where higher numbers of the cyclopoid copepods Oithona spp., Corycaeus spp. and Oncaea spp., and the harpacticoid Microsetella spp. were found. |
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